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<br />"- <br />Q) 12 __ ___ _ .._____________ .,_,_________"__..m____"" ,_______________.,__________._____"'____~__________~__ - 670 <br />...... <br />Q) 10 1994 566 <br />E , <br />U f .. <br />8 I 453 <br />.0 <br />:J 6 - 340 <br />u . . <br /> . . <br />- <br />~ 4 227 <br />Q) <br />~ 2 ....... zooplankton 113 <br />~ 0 :........................ 0 <br /> 70 670 <br /> 1995 -- <br /> 60 566 en <br />"- 50 E <br />Q) 453 u <br /> -- <br />~ 40 Q) <br />~ 340 C) <br />Q) 30 "- <br />.0 227 co <br />E 20 .c <br /> u <br />:J 113 .~ <br />Z 10 0 <br /> 0 0 <br /> 70 670 <br /> 60 1996 566 <br />"- 50 453 <br />Q) <br />~ 40 <br />~ 340 <br />Q) 30 ............ <br />.0 227 <br />E 20 ............ '..- .... <br />:J zooplankton 113 <br />z 10 <br /> 0 0 <br /> 10 20 30 10 20 30 10 20 30 10 20 30 10 20 30 10 20 <br /> May Jun Jul Aug Sep Oct <br /> <br />Figure 17.Comparison of zooplankton collected (dotted line) from Old Charley Wash in the spring and summer between 1994 and 1996 <br />with river discharge (light solid line) measured in Jensen and the duration of larval razorback sucker collected in the middle Green River <br />(heavy horizontal line). The larval razorback duration line is located at the 447 cms scale to compare larval presence with floodplain <br />connection, and the flows in which most backwaters appear (109 cms) is noted with an arrowhead. <br />